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Guinea

(Guinee), Guinea's desired pebble Populaire (Republique Populaire et Revolutionnaire de Guinee), - State-Wax. Africa. It borders on C. C Soregal, on C. and C.-B. C Mali, on B. With the shore of the clone, on Yu. With Liberia, on Yu.-Z. CO Sierra Leone, on C.-Z. C Guinea-Bissau. HA Z. is washed by Atlantic. OK. Pl. 245.8 thousand km 2. HAC. 6.4 million people (1980,). It is divided into 29 administrative P-new. Soligitsa - Kryakri. Ofić. Language is French. Monetary unit - Sili. G. is included in the Argration of AFR. Unity (OAE), is a member of the economy. Communities of the West African countries (1975).
What is the characteristic of the illness. GDP is $ 800 million (at current prices, 1978). B of its structure for a fraction c. The X-Wa accounts for 21%, Prom-STI 25% (including the share of mining 18%). B Fuel and Energy Structure. Balance share of oil 98%, hydropower 2% (1979). Without the length of the highway 30.0 thousand km, the length of it. d. 1.1 thousand km (1980). Rupual mor. Ports - Konakri, Kamsar. O. A. Lykina.
Nature. B relief is distinguished: the inntlantic (highest. Up to 70 m), step-down-jalon plateau (high. 150-1300 m, maximum - 1538 m), Entroduction-Guinea (CP. Height OK. 800 m, Maximum - 1752 m ) and the plains of the first HEGER (high. 300-400 m). Klimat Equatorial-monsoon, hot, summer-wet. CP. Temp-PA of the warmer month (March or April) 27-30 ° C, the coldest (August) 24-26 ° C. The annual amount of precipitation on the coast of St. 4000 mm, in the remaining P-ns 1200-1500 mm. The most means rivers: Heger, Kogon, Hunta, Fatala, Konkur (the mouth of some rivers shipping). Lesosanny, southern prevail prevails. The desperial-Guinean elevation is covered with wet equatorial dense forests (approx. 4% terr.), On Z. Countries - Mangra.
Geological Strip. Located on Z. African platform. HA B., Yu.-B. and Yu.-Z. Leono-Liberian, center. Parts of the country - southern. Synecleses of Taudenni and the deflection of Pokel, on Z. - West Guinea. The Leono-Liberian shield is complicated by the formations of Archey (GNEY, quartzites, metamorphic ultrasound breeds, granites) and bottom. Proterezhoya (, gneus, quartzites, limestone breeds, grains, volcanics and granite breaking them). With ferrous quartzits of Archey, large metamorphogenic massers are connected. ore. South. The board of syclipses of the Taudenni is formed by generous-hazing proteozoic carbonate-terrific strata, the Mrouting of limestone is confined. The deflection of the fleece is made by proteozoic, crumpled in carbonate-terrific precipitation and effusion; There are metamorphic. breeds (slates, quartzites), among the to-rye there are hematitic ores; There are functions. West-Guinean syneclizes are described by the rolling rocks of the Ordovic, Silura and Devon (sandstones, aleurolites, argillites). The manifestations of manganese, in Devonian and Silurian rocks - small Mr. sediment micro-oolithic jams are localized. ore. Koinozoic (, Suglinki, and pebbles) are developed on Atlantic. The coast (Mor. terraces, beaches, braids) and by the valleys of the numerous. rivers. K coastal mor. The formations are dedicated to small zircon, Ilmenit, Rutila, Monazita, Mr. Kaolina, manifestations of lignites and phosphorites, to alluvia river terraces - gold and diamonds. Rannoproterozoic magmatism associated indigenous (core) Mr. Gold, with Latezozoic - kimberlitic dyes and tubes, ne-ry c prom. Diamond content. Dunites, Gabbro-Norites, Mesozoic, less frequently of Paleozoic age, forming arrays, sillas and dikes are widely developed. Mesocynezoic weathered with large mrenines of bauxite, jerks, widespread. ore, a nickel and chromium ore. C. C. Prokofiev.
Hydrogeology. Underground water on terr. G. have limited distribution. ONS Groundwater reserves are associated with alluvium of large PP valleys. Heger, Tominne et al. (Specific flow rate 1-2 l / c, sometimes up to 4 l / c) or with fractured rocks. Parts of weathering in reduced areas of relief (0.1-1.5 l / c). B indigenous breeds in the OSN. Unzable, with the exception of the sandstones of the Ordovic, opened with wells with specific flows of 6-7 l / c. Underground water - ultrapresses, with mineralization up to 0.3 g / l, hydrocarbonate, and mixed cationic composition. Underground waters are performed only in wet seasons. B Dry periods of river costs are sharply reduced, most sources disappear, which creates difficulties in water supply. P. I. TKACHENKO.
Minerals. G. is rich in boxcites and jerseys. ores (Table 1).

There are small grams of gold, diamonds, chromium ores, nickel, ilmenite, zircon, rutile, monazita, beryl, limestone and graphite slates.
ONS Mr. Pyd associated with ferrous quartzits of Archeye focused in the P-sticks of the HEMB ridges (reserves of 2 billion tons, iron content of 60%) and Cymanda (7 billion tons, 60%). B zap. Parts of the Minor Mr. Zack. (hematitic) ores are known to Yu. From the city of Forekaria and Bass. p. Tomine (microloan ores). HA P-OS Kalum Mr. ores (explored reserves 1476 million tons, Fe 51.5%) are confined to the lativity of weathering cortex in the rocks of ultrasound and main compositions; There are also small fields of nickel and chromium ore deposits.
Po reserves of Boxitov G. occupies 1-e place among industrialized capitalist. and developing countries (approx. 40% of reserves, 1980). Extra Mr. focused on the center. and zap. Parts of the country in bauxalone P-na: bokeh-gallow (main. Mr.: Sinthioura, explored reserves 501 million tons, the content of Al 2 O 3 46.6%; Dian-Dian, 300 million tons, St. 40% ; Dubular Tagurata, 431 million tons, 40%); Fria-City (Manga, 507 million tons, 41.3%; Tioreor, 268 million tons, 49.6%); Dongel-Sigor (OPE-LITI, 250 million tons, 47%); Bantinyl (Kasagi, 154 million tons, 46.3%); Dubol (telly-act, 217 million tons, 40-45%); TUGE (Pantiolo, 390 million tons, 40-45%; kox, 391 million tons, 40-45%); Debel - Kindia (debt, 44.4 million tons, St. 40%). Also known Mr. Bauxites on B. Countries, near XP. HEANDAN BANK. The genesis is divided into latitite and polygenic (latically sediment); OSN. Rudny - Gibbsit.
ONS Gold reserves dedicated to quartz veins are divorced to the east. Parts and small parts (Mr.; TEnetso, reserves 24 tons, the content of Au 0.4 g / m 3; Sigirini-Ko, 1 t, 17.4 g / m 3). Mal diamonds are located on Y.-B countries in Pools p. Baul, Macon, Diani. They are confined to kimberlite tubes (0.6-4.5 car / m 3), dikes and small alluvial places (0.2-4.8 car / m 3). Possessing Ilmenite, Zircon, Rutila and Monacite (Mr. Berga and others) focused along the coast of the ocean in the sediments of the first Mor. Terraces, Mor. Kos and beaches. Width off. Rosyper 250-300 m, Length OK. 1.5 km. CP. The total content of valuable minerals is 40-60 kg / m 3. Reserves 20-76 thousand tons are also estimated by 20-76 thousand tons (for example, on Mr. Berga, the total reserves of Ilmenit 60 thousand tons, a zircon of 10 thousand tons, rutila 5 thousand tons). Known small Mr. (Kurund, Amaraya, Lebekistan) of limestone, a also Berylla and Kaolina (near the city of Kay), graphite shale (near pos. Lola). C. C. Prokofiev.
Mining. What is characteristic. Mining. Prom-ST is one of the leading industries, the K-Rui accounts for 60% of those employed in the prom, 87% of the gross volume of prom. Products. (Paschennaya Osn. Objects Minskob. Prom-sch is shown on the map.) Horn Gorn. Prom-STI - Bokuxte Mining (Table 2).




B country There are 3 baxitodobes. Firms: "Compagnie Des Bauxites De Guinee" (49% of the shares belong to Gosv), mixed by the "FRIGUIA" (49% of the shares belong to the State Wu), "Office Des Bauxites De Kindia" (entirely belongs to the state). Minskob products. Prom-st provides 97% of the cost of exports. Countdown in Osn. exported bauxites (St. 10 million tons, of which 2.9 million tons in the United States, Kanadu 0.85 million tons, in socialist. Countries 4.1 million tons) and (0.6 million tons), Imports petroleum products (283 thousand tons), a small amount of coal builds. Materials (1978). GL Trading partners in the countries of the UES, USA, CCCP. O. A. Lykina, C. C. Prokofiev.
Bauxite-producing prom.. PO bouxite production is 2-e. Place (17%), according to their exports 1-E place (30%) among industrialized capitalist. and developing countries (1979). Boxitis exports in 1978 compared with 1970 (811 thousand tons) increased by more than 10 times (10.3 million tons). M-Bowls are developed by the open method with the use of drilling work. The shape of the deposits is plastic (6-12 m reservoirs), the power of the opening in CP. 0.5 m. B p-non-Fria-City (Mr. Kimbo) Development is conducted with 1959. Production. Career Power SV. 2 million tons of ore per year. Recycling C 1960 - on the alumina Z-de in the city of Fria, alumina 85-90% (1978), production of Sv. 600 thousand tons (1980). Dresses d. (for. 145 km) and through the port of Kari. Mr. in the Chang, in the P-non-bokeh-gallow is developed by C 1973. Production. Career Power 9 million tons. D. (DL. 138 km) enters the enrich. F-ku to the port of Kamsar and then transported by rudders with displacement of 45-60 thousand tons. Mining in P-non-debt-Kindia (Mr. Debel) began with con. 70-X. open way. The Parier is built with the participation of owls. specialists. Production. Career power 2.5 million tondes per year. PUDU PO d. (for. 98 km) is delivered to the port of Konakri. For the development of new Mures Bokuxites, 3 open-mining enterprises were created: on the P-on TUGE (design capacity of 8 million tons of ore per year), on Mr. AEEEE in P-Non Bokeh-Gaow (9 million Tues per year), where it is planned to build an alumina z-yes with a capacity of 1.2 million tons and aluminum z-yes, and on the Mrenions of P-for Dubol (6.5 million tons of ore per year), on the basis of bauxite It is supposed to build an alumina z-d. The increase in the producer of alumina is constrained by the difficulties with electricity, which will be, possibly overcome with the commissioning of the hydroelectric power station on P. Konkur.
Mining other minerals. Mining jerk Ruds in the city began in 1953 and until 1967 was developed by Mr. Kalum. Designed the development of large msions. Rud on Yu.-b. in gg HEMBA and Cymanda. Complete development of these ms is planned after page. d. from the city of Konakri to the border with Liberia.
Diamond mining for terr. G. Began in the 30s. And conducted by private companies and prospectors. B Nach. 60-X. Almazodob. Enterprises are nationalized in CEP. 70-X. Prom. Mining is suspended due to reserves and the lack of new will enrich. equipment. EE renewed is planned.
Gold mining to terr. G. has been published by the handicraft in the beginning of the 20th century. Europe. Entrepreneurs have repeatedly tried to establish the development of drags (for example, 218 kg of gold were produced in 1909-14. ONNO due to insignificance of stocks industrial mining is discontinued.
Geological service. Personnel training. Organization of mining geology. Works in G. is carried out by Min-in Horn. Affairs and geology. Gorno-Geol. Frames are preparing at Gorno-Geol. F -E (in the town of Boke) Polytechnic. In-ta in Konakri. Literature : Mihalov B. M., Geology and Western regions of the Liberian Shield, M., 1969; Prokofiev C. C., Tashkin B. I., Geological and Economic Assessment of Boxitite Resources Guinea, M., 1979. C. C. Prokofiev.

Mountain Encyclopedia. - M.: Soviet Encyclopedia. Edited by E. A. Kozlovsky. 1984-1991 .

Watch what is "Guinea" in other dictionaries:

1) The Republic of Guinea, state at 3. Africa. The name of the State Guinea (Guinee) is taken by the name of large geogr. oblast Africa Guinea, which from the XIV century. Indicated to Europe. Maps in Ganua, Ginya, A with the XV century. like guinea. Most likely ... ... Geographic Encyclopedia

Guinea - Guinea. In the upper reaches Niger. Guinea (Gwinean Republic), the state in West Africa is washed by the Atlantic Ocean. Area 246 thousand km2. Population of 7.2 million people, Fulbe, Malinka, Susu, etc. The official language is French. Over 80% ... ... Illustrated Encyclopedic Dictionary

- (The Republic of Guinea), the state in West Africa is washed by the Atlantic Ocean. Area 246 thousand km2. Population of 7.2 million people, Fulbe, Malinka, Susu, etc. The official language is French. Over 80% of the population of Muslims, about 1% ... ... Modern encyclopedia

REPUBLIQUE DE GUINE (REPUBLIQUE DE GUINE), State in Zap. Africa. 246 thousand km & sup2. Population of 7.4 million people (1993); Fulbe, Malinka, Susu and others. Urban population 25.6% (1990). Official language is French. Believers 85% Muslim, ... ... Big Encyclopedic Dictionary

GUINEA - (Guinee), the Republic of Guinea (Republique de Guinee), the state in West Africa. Pl. 245.8 t. Km2. Us. sv. 5 million h. (1982). Capital Conakry (700 tons, 1982). Prior to the proclamation of independence in 1958, the ownership of France. G.GP. Country with ... ... Demographic Encyclopedic Dictionary

GUINEA - territory of 246 thousand k.km, population of 7 million years old (1986). Agriculture plays a major role in the country's economy. 70% of the population is employed in this industry. Home Food Culture Fig. Main areas of livestock breeding feet Jalon, top ... World shepherdie

GUINEA
The Republic of Guinea, the state in West Africa has access to the coast of the Atlantic Ocean. It borders in the north-west with Guinea-Bissau, in the north - with Senegal, in the north and east - from Mali, in the south-east - with Côte d "Ivoire, in the south - with Liberia and Sierra Leone. Area 245.9 thousand square meters. km, population population - 7673 thousand people (1998). Capital is the city of Conakry (800 thousand inhabitants, 1996). Other large cities - Kankan, Kindia, Labe, Sigiri.

Guinea. Capital - Conakry. The population is 7673 thousand people (1998). Population density - 31 people per 1 sq. M. km. City population - 23%, rural - 77%. Area - 245.9 thousand square meters. km. The highest point is Mount Horba (1752 m). The main languages \u200b\u200bare Fulbe, Malinka, Susu, French (official). Major religions - Islam, local traditional beliefs. Administrative and territorial division - 8 provinces. Monetary unit: Guinean franc \u003d 100 centimam. National holiday: Independence Day - October 2. State Anthem: "Freedom".

At the end of the 19th century Guinea was conquered by France and included in the French West Africa. After the Second World War in Guinea, the massive national liberation movement was gained strength, which headed the second of the tour. At the referendum on September 28, 1958, on the project of a new French Constitution, almost all of the population of Guinea supported the anticolonial course. The Guinean rejected the idea of \u200b\u200bincorporating the country into the French community, choosing a path of complete independence from the metropolis. On October 2, 1958, the independent Guinea Republic was proclaimed. In response, France immediately interrupted all ties with Guinea and recalled all French personnel from there. Independent Guinea, led by the President of the second of the tour, who occupied this post until death in 1984, was one of the radical African states standing in the positions of Panaforkanism.
Nature. The territory of Guinea is divided into four physico-geographical areas. The first one, located in the West of the country, is Lower, or Primorskaya, Guinea - is a flat lowland wide up to 32 km wide, with heights less than 150 m above U.M. The coastal wetland is covered with mangrove thickets, dense rocks overlook the surface only in the area of \u200b\u200bConakry. Lower Guinea is an area of \u200b\u200bcommerce-export farming. Here are mostly representatives of the people of Susu. The cutting lowland river Cogon, Fatala and the competitor originates in the deep valleys of the second district - Middle Guinea. Here, the sandstone array of Futa-Dzallo with tops 1200-1400 m crosses the country from north to south. The highest point of the plateau, located north of Lab, is Mount Tep (1538 m). Middle Guinea is distinguished by the predominance of Savann landscapes, there are mountain meadows in the highest places. The area is populated by the people of Fulbe. The prevailing occupation of the population is animal husbandry. East of the Massif Futa-Dzallo, on the plains in the upper current pool R.Niger, is the top Guinea. This is the Savannan area populated mainly by Malinka farmers. Forest Guinea, located in the south-east of the country, occupies part of the North-Guinea hill with small arrays of the remaining mountains. Here, near the border with Liberia in the mountains of Himba is the highest point of Guinea (1752 m). In this area, the background is made up of savanna, in some areas, especially on river valleys, tropical forests have been preserved. In Forest Guinea, there are many small nations who are engaged in agriculture. For the climate of Guinea, a clearly pronounced contrast between the wet season, which is continuing from May to October (and on the coast - longer than on the plains of the northeast) and the dry season, when the hot wind is blowing from the northeast - Harmathan. With the exception of its northern part, the seaside lowland is reliably protected by mountains from dry wind. Wet southwestern winds bring abundant precipitation, which fall out on the western slopes of the mountains. Conakry district is characterized by an average annual precipitation of 4300 mm, of which 4000 mm fall on the wet season. In the inner areas falls on average 1300 mm per year. High temperatures prevail throughout the year, rarely dropped below 15 ° C, and sometimes reaching 38 ° C. The greatest population density is characterized by an array of Futa-Jalon, where a large cattle, sheep and goats graze, and in fertile valleys grow Different agricultural crops. The export value is coffee, which is produced in medium and upper guinea, as well as bananas grown on seaside lowlands and in the valleys near the railway. In a number of coastal locations, mangrove thickets were cleared under rice fields.
Population. In Guinea, there lives a lot of ethnic groups, the largest of them are peoples speaking Manda (Malinka, Susu, etc.) and Fulbe. Fulbe accounted for 35% of the population, Malinka - 30% and Susu - 13%. The rest: scrap (volume), gerza, kisi, dlalonka, etc. - in aggregate are 22%. Local languages \u200b\u200bare so different that even those who live in the neighboring regions of the Guinea cannot always understand each other. The official language is French, but they own not all residents of the country own (especially in rural areas). Malinka lives in the inner regions of the country, mainly in the R.Niger pool, Susu (presumably the most ancient residents of Savannan) - on the coast, including the strip between Conakry and Kindia. The main occupation of the madeyagiden peoples that make up about half of the population of the country - agriculture. Fulbe's militant cattlemen, which appeared in these places in the 16th century, inhabit mainly the central part of the country - the Array of Futa Jalon. A number of small ethnic groups are common on the coast, on the western slopes of Plateau Futa-Dzallo and in Forest Guinea. The old enhancement between the rural population speaking Manda, and Fulbe's Celebrations, which has currently accepted the form of rivalry for political hegemony in the country. Approximately 90% of Guinsev - Muslims. Most of the rest are adherents of local traditional beliefs and cults. Although the first Christian missions were founded on the territory of modern Guinea at the 19th century, the number of Christians is slightly.
Political system. For more than a quarter of a century Guinea ruled the second round. He headed the Democratic Party of Guinea (DPG) and in October 1958 led the country to independence and was its president until 1984. After the death of the Turing, the group of military personnel headed by Colonel Lance Conte captured power in the country in April 1984. As a result, the Constitution was suspended, The rules and mass community organizations operating under the auspices of this party were dissolved in the conditions of unionarity. The country's Office took over the Military Committee of the National Renaissance. The first Constitution of Free Guinea endowed the president by the broad authority of the head of the country and the head of government. The President was elected at the general election for a period of 7 years. In 1972, the post of prime minister was approved, which was appointed president. The legislative authority, the National Assembly, were limited powers. All of his 210 deputies were elected at a single list of candidates. In accordance with the amendment adopted in 1974, the Congress of DPG proclaimed the "Higher State Body". DPGs sought to monopolize power so that a political, social and economic modernization in the country should be in the country. The conductor of transformations should have become a well-organized and disciplined batch whose cells were created in each village. Membership in local party, trade union, female and youth organizations was practically mandatory. The top of the powerful pyramid was the Supreme Executive Party Origin - Politburo DPG. Nevertheless, dissatisfaction increased in the country, in response, the authorities held a number of cleansing in the state apparatus and the army. In 1978, after mass unrest, during which several provincial governors died, measures were taken to restore the confidence of the population to the DPG and the Government. Regular conferences have been held for activists of local trade union, female and youth organizations. The general elections began to choose governors of provinces and managers of district party organizations, who previously appointed party bodies. In 1984, the military headed by Colonel L. Konte came to power. In 1990, a new constitution was adopted, providing for the creation of a multi-party system. In 1993, L. Konte was elected president of the country. In 1997, Guinean's armed forces numbered ok. 9.7 thousand people. In the folk police served 9.2 thousand people. Greater assistance in the creation and equipping of the Guinea army was provided by the USSR and China. In the field of foreign policy, independent Guinea officially proclaimed the Non-Aligned course. In 1958-1961 and from the mid-1960s to mid-1970s, Guinea supported closer relations with the USSR and other socialist countries than with neighboring African states and the West countries. Under the pretext of the participation of France, Franco-Guinean diplomatic relations were interrupted against the Government of Guinea in 1965. In the mid-1970s, Guinea strengthened relations with countries in Africa, the Middle East and the West. In 1976, diplomatic relations with France were restored. Guinea is a member of the UN, the Organization of African Unity (OAU), the Economic Community of West African countries (ECOWAS). A serious threat to economic development and political stability of Guinea creates, especially in the last decade of the 20th century, a continuous flow of refugees from neighboring Liberia and Sierra Leone, where civil wars do not stop.
Economy. Guinea is rich in natural resources. In the country there are reserves of minerals, large areas of fertile lands, rivers have a large hydropower potential. Guinea has the world's largest bauxite deposits. The mining industry brings almost the entire extension from exports to the state budget. However, the main occupation of the population remains a rural natural or fine-friendly economy. Industry is poorly developed, although its share in GDP is constantly growing. Many profitable economic activities in Guinea are under state control. Within 15 years, after the proclamation of independence, the government gradually eliminated private trading. Only state trade organizations functioned, and the peasants were obliged to implement their products through a network of state stores. After the riots, riding around the country in 1979, the government was forced to cancel the ban on private trading. Large industrial enterprises, especially working for export, remained owned by the state.
Agriculture. About 80% of Guinean's population is occupied in agriculture. The main cultures are rice, maniacs and corn, they also form the basis of the food diet of the Guinean. The peasants are breeding cattle, sheep, goats and poultry. The country does not provide itself with food and is forced to import rice, sugar and dairy products. In the early 1980s, only 1/7 of lands suitable for processing, labor productivity remained low due to the backward material and technical base of agriculture and the lack of incentives for the maintenance of commercial economy. The main export cultures of Guinea are bananas, a chocolate tree, oilseed palm, pineapples and peanuts - grow mainly on plantations. After 1958, the collection and export of these crops was significantly reduced due to the departure of European specialists and the loss of French markets. In the early 1980s, the production of export agricultural products (except bananas) remained low.
Mining industry. In Guinea, Bokuxite Bokok, Tight, Fria, Kindia, Debel, and others are open in Guinea, the 2/3 of the world's bossite reserves (20 billion tons), and this country - the second largest supplier of raw materials for aluminum, focused in Guinea Industry on the global market (more than 12 million tons per year). In 1993, the share of production of the mining industry in the cost of exports was approx. 86%, but in 1994-1995 decreased to 78%. The development of most mineral deposits is engaged in joint ventures established by foreign consortia and the Government of Guinea, which, as a rule, owns 49% of the shares of such enterprises. In the early 1980s, three bouxite mining enterprises operated in the country - in Kindia (fully belongs to the state), Fria (property of the Fryigia consortium) and bokeh (belongs to the mixed society "Bauxit de Gin"). In 1995, the total mining of bauxite amounted to 13.6 million tons. Since the second half of the 1980s, industrial gold mining is carried out - up to 1 ton year, which provides 20% of the cost of exports. The explored gold reserves only in the upper guinea are 500 tons. Guinea has considerable in stocks of diamonds - more than 100 million carats. Diamond mining is conducted in the south of the country (200 thousand carats per year). The explored reserves of high-quality iron ore in the mountains of Himba are approx. 12 billion tons (in 1997 mining has not yet started). Guinea also has the reserves of uranium ore and copper.
Manufacturing industry. The industrial sector of the economy began to develop only after the conquest of independence. In the early 1980s, the industrial sector gave only 5% of national income. In 1995, 0.6% of the able-bodied population was employed in industry. At a large plant in Fria, aluminum is paid for export. Other industries are represented by food, textile, cement industry, as well as building materials.
Transport. Of 12.4 thousand km of roads, only 5 thousand km have a solid coating. Railways associate Conakry with Cacano and Fria, as well as bokeh and Kamsar. In 1997, the Slovak company received a contract for the modernization of the railway track between Conakry and Kalkan. In 1996, Iranian government declared its readiness to build a railway connecting Conakry with rich boxes Dubol-Tuga. The largest port of Conakry has a natural deepwater harbor. In 1973, a new port was built in Camsara.
Trade and investment. Throughout the 1960s - early 1970s, the Trade Balance of Guinea comes down with a deficit. However, from the mid-1970s, the trade balance has become positive, mainly due to the growth of income from bauxite mining. In 1991, the situation returned to the previous state. In 1993, the value of imports amounted to $ 731 million, and exports - $ 665 million. If in 1993-1995, Guinean's trade balance was deficient, then in 1996 he had an active balance in the amount of 111 million dollars. Share bauxite and alumina in export The receipts decreased from 65% in 1993 to 54% in 1995. Other export articles: diamonds, gold, coffee, bananas, oil palm products, peanuts and pineapples. Main trading partners Guinea - France, other countries of Western Europe and the United States.
Finance and banking. In 1960, Guinea came out of the French franc zone and the West African Monetary Union. Today she has its own currency, whose emissions are engaged in the central bank. In October 1972, Guinea replaced Franc with a new monetary unit - Sili, but in 1985, Frank was introduced into the money circulation. Central Bank Guinea controls financial institutions that are engaged in commercial banking. Guinea has a huge external debt and there are practically no reserves of foreign currency.
Popular education. For children aged 7 to 12 years, school studies are free and required. In 1993 approx. 46% of the children attended primary schools and approx. 12% - average. Almost a third of students amounted to girls. In elementary school, focus on the acquisition of agricultural skills, emphasis is on training in technical specialties. In Kankane and Conakry there are polytechnic institutions. Over the years of independence, the level of literacy of the population has significantly increased. If in 1965 only 10% of adults were able to read and write, then in 1995 their share increased to about 35%.
History. In 10-11 centuries. Most of the northeast of modern Guinea was part of Ghana. On the presence of Sigiri, a part of Ghana Ghana was probably mined, which in the cities of Sahel exchanged on the salt and other goods from North Africa. At 12 in. The Ghana Empire broke up, and in the 13th century. In her place, an empire of Mali, created by the people of Malinka, originated. Among the nobility and citizens widely spread Islam. Before the beginning of the 16th century Mali remained a powerful force in the region. Later, the Songy Empire Gao in the East and the state created by Fulbe, the state of the Tener - in the West, captured the significant part of the territory of Mali. In the middle of the 17th century Bambara from Saga overthrew the emperor Malinka. By that time, the Trade Center moved to the coast, where the acute competition between Portuguese, British and French workers unfolded. However, in this part of the West African coast of the slave, it was less common than on the coast of Nigeria, Dagomey and Senegal. After the official ban on the worker in the early 19th century. The coastal areas of modern Guinea continued to attract traders in a living product, since a strongly rugged coastline provided reliable shelters for the workers' ships, which were hunting British warships. In the middle of the 19th century Peanuts, palm oil, skins and rubber came to replace the slave trade. European merchants settled in several factors and paid tribute to leaders of local tribes. Attempts by leaders to increase the size of Dani ended with the fact that France in 1849 installed its protectorate over the side area. At the beginning of the 18th century. The powerful state of Fulbe arose on the territory of Plateau Futa-Dzallo. Its state religion became Islam, which then spread among the inhabitants of coastal areas, many of which paid tribute to the leaders of Fulbe. Further development of European trafficking and the creation of new reference points on the coast in the middle of 19 V. He led to friction between the French and the leaders of Fulbe, which in 1861 managed to convince the French protectorate over bokeh. A few years earlier, a military religious reformer from East Senegal Haj Omar settled in Futa-Jalon. By 1848, his popularity among the local population grew so much that it became anxiety from the leaders of Fulbe. Haj Omar was forced to move in Dingirae, where he declared Jihad (sacred war) in the territory of Western Sudan, primarily the kingdoms of Sega and Masina. In 1864, in the battle with warriors, Masina Haj Omar died, and his place was taken by the son of Ahmad. In 1881, he concluded a contract with the French, according to which the territory on the left bank of Niger was transferred to Tombukta under the French Protector. Later, Ahmad tried to abandon this contract, but in 1891-1893 he was removed from power by the French. The longest and decisive resistance to the French colonizers had a Samori tour. Malinka on ethnicity, he in 1879 captured Kankan and created a Muslim state southeast of Sigari. In 1887 and 1890, the French concluded a friendship contract with Samori, but then denounced them, and military actions resumed. In 1898, the French captured Samori Tour near Mana in the west of the modern Côte d "Ivoire and sent a link where he died. The Samori round capture marked the end of the organized resistance of the Africans to the French invaders in the territory of modern Guinea, although the natural speeches of the Guineans did not stop until the beginning First World War. In 1895, Guinea was included in the French West Africa, and in 1904, after the British were transferred to the French of Los, the borders of the colony were established. During the French colonial government, the Guinean was deprived of elementary political rights, paid a pure tax They were mobilized for unpaid forced work and military service. In 1946, France went to the creation in Guinea of \u200b\u200bthe electoral territorial assembly in Guinea and gradually softened property and educational censes to participate in the vote. In 1957, all adult populations of the colony could participate in the elections, the Government Council was created. - Territoria The executive body, which consisted of Gwinetsev. The influence of the Democratic Party of Guinea (DPG), the mass political organization, headed by the trade union leader of the second of the tour, was rapidly increased. Thanks to the propaganda work of the party activists in 1958, almost the entire population of Guinea spoke in a referendum against the new French Constitution and for the exit of the country from the French Community. As a result, on October 2, 1958, Guinea gained independence. The choice of Guinean in favor of independence turned into a loss of French economic assistance and investment, a guaranteed market for the sales of export products and technical assistance to qualified specialists. The acute need for economic and technical assistance forced the new government to ask for help from the USSR and China, which led to even greater insulation of Guinea from France and its allies. In 1965, Guinea ruined diplomatic relations with France, accusing it in participating in the conspiracy in order to overthrow the Guinea government. By the end of the 1960s, Guinea has established relations with a number of Western states, which was largely due to the interest of the country's leadership in foreign investment. However, the nationalization of trade and the agricultural sector turned out to be held in all sectors of the Guinea economy, except for the mining. Although the second itself retained his authority among the population, the government rate became less popular, and many thousands of Guineans emigrated. In November 1970, Guinean emigrants, which were in opposition to the regime of the tour, took part in the armed invasion of Guinea, which was organized with the support of Portugal. This action pursued two main objectives: the overthrow of the government of the second of the tour and defeat of the Baz partisans, who fought for the liberation of Portuguese Guinea (now - Guinea-Bissau). The rebels were quickly broken. After a failed attempt at aggression, mass purges were carried out in the state apparatus and the Armed Forces of Guinea. In August 1977, a wave of riots swept around the cities, during which several provincial governors appointed by DPG were killed. After these events, the policy of the Guinea leadership changed dramatically. In the late 1970s, political repression was weakened, the masses were able to participate in public life, private trade was permitted. Guinea's relationship with neighboring African states and West countries has improved. In 1976, diplomatic relations with France were restored. The second of the tour died on March 26, 1984, and already on April 3, 1984, the group of servicemen, headed by Colonel Lansana Conte, carried out a bloodless coup. Military authorities dissolved DPGs, freed all political prisoners. Economic reforms of the define regime have not brought positive results. In 1991, a new constitution was adopted, providing for the creation of a transitional government, and then a multiparty republic. As a first step towards the transition to civilian government, the activities of political parties were legalized. According to the results of the multiparty elections in the history of the country's first in the history of the country, Conte was elected president. The 1995 Parliamentary Elections, accompanied by numerous clashes and acts of violence, won a batch of unity and progress, headed by Conte. In 1996, Kontte appointed a new Cabinet of Ministers and introduced the post of Prime Minister appointed by the President. The Government Conte laid the task more vigorously to conduct a program of economic reforms, providing a reduction in government spending, combating corruption and improving the efficiency of the tax system.

The encyclopedia of the colley. - Open Society. 2000 .

6 - /: 99-y / "- Mr

Minister of Commercial and Professional Education of the Russian Federation, Ministry of Higher Education of the Republic of Guinea, Moscow State Geological Exploration Academy of Concilia University

Bubakar owl

% Conditions for the formation of bauxite deposits

Bokeh Kindia-Tuga triangle, geochemical inhomogeneity of bauxite deposits and optimizing exploration network parameters (Guinea).

Dissertation thesis on the degree of candidate of geological and mineralogical sciences

in the specialty: "04.00.11-geology, searches and intelligence of ore and non-metallic minerals; Metal Metal

Moscow 1999.

Republique de Guinee.

tRAVAIL-JUSTICE-SOLIDARITE. ■

MiniseRe De L "ENSEIGNEMENT SUPÉRIEUR ET DE LA RECHERCHE SCIENTFIQUE MINISTERE DE L" ENSEIGNEMENT GENERALE ET PROFESSIONNEL DE LA RUSSIE UNIRERSITÉ GAMAL ABDEL NASSER DE CONAKRY ACADEMIE NATIONALE DE PROSPECTION GÉOLOGIQUE DE MOSCOU

Boubacar SOW Conditions De La Formation Des Gisements De Bauxite Du Triangle Boke-Kindia-Tougue, L "Heterogeneite Geochimique Des Gites Bauxitiques et L" Optimisation Des Paramets Du Maille de Prospection (Guinee).

These de Candidat Es Sciencees Geologo-Mineralogiques

Conakry-Moscou 1999

C "EST POUR MOI UN RÉEL PLAISIR DE REMERCIER APRèS CE TRAVAIL RUDE ET PÉNIBLE TOUS CEUX QUI DE PRAIBU OU DE LOIN, ONT CONTRIBUÉ À L" ÉLABORATION DE CETTE THZEE.

Je Tiens à Remercier La Direction Du Center Minier, Surtaut Mr. Bangoura et Mr. CONTE AINSI QUE LEURS COLLABORATEURS DE LA DIVISION ARCHIVES ET Documentation.

Je Remercie Également La Direction Nationale De La Recherche Géologique Pour Leurs Conseils.

Toute Ma Reconnaissance à la Division Géologique De La Société Des Bauxites De Kindia (SBK) De Débélé Qui M "A Réellement Facilité Les Recherches.

J "Adresse Mes Sentiments de Gratitude:

Aux Professseurs De L "Université De Conakry et Singulièrement Ceux De La Faculté Des Whiteces Pour Leurs Sages Conseils.

Au Pr. Nanamoudou Magassoubé Qui M "A Encouragé Dépuis 1994 à Profiter De La Présence Du PR Gleb Victorov Afin de Finir Ma Thèse.

Au Dr Thierno Amar Dialo Et Son Collaborateur Mr. Souleymane Bah Pour La Saisie de Ce Travail.

Je Me Souviendrai Pour Toujours du Soutien Moral et matériel des Autorités du Décanat De La Faculté des Sciencees et du Rectorat De L "Université De Conakry Dans L" élaboration de Ce Travail.

J "Adresse Singulièrement Mes Sentiments De Gratitude ET De Reconnaissance:

Au Pr. Gleg Victorov Qui A Été Mon Professeur et mon Consultant De Mémoire De Fin D "études supérieres en 1978 et, aujourd" HUI Encore Est L "Un de Mes Consultants à Cette Thèse.

Au Pr. Bortntkov A.J. QUI FUT MON PROFESSEUR LORS DE MES ÉTUDES SUPÉRIEURES ET QUI EST AUSSI MON CONSULTANT à Cette Thèse.

A Mon Père et à ma Mère, Je Dédie Ce Travail. ENFIN À TOUS CEUX QUI DE PRèS OU DE LOIN M ONT APPORTÉ LEUR SOUTIN, JE DIS Merci.

Relevance of the topic. Boxites are the main mineral ^ Raw Guinea. In their reserves, Guinea occupies a leading place in the world. Currently, several large deposits are intensively developed in the country, new, previously explored facilities are involved, search and exploration are actively conducted.

The largest and rich in the content of alumina bauxite deposits are concentrated in the triangle of bokeh-Kindia-Tug. However, the study of the complex structure with low contents and small reserves, located outside of this area, are often involved in the study.

At the same time, the prospects for identifying rich fields in the triangle of Bokeh Kindia-Tuga are far from being exhausted. This area is characterized by a unique combination of natural factors favorable for fish and is the most promising.

In the structure of bauxite deposits, horizontal and vertical zonality often noted, insufficiently taken into account in the geological and exploration work. Accounting for zonality to substantiate the optimal densities and configuration of the exploration network would lead to significant reduction in exploration costs.

These complex and relevant issues for the economy of Guinea are solved by the author with the involvement of the latest data of cosmic photography and methods of mathematical statistics.

Objectives and objectives of research. The purpose of the study is to show that the placement of large-scale alumina in the contents of Bokuxite deposits in the Bokexites triangle is due to the unique combination of a complex of climate and geological conditions favorable for bauxilite formation, and that this area is the most promising and must be mastered in First of all. The second aspect is to establish the features of the spatial distribution of the parameters of the mineralization inside

boxite deposits and choosing this basis for optimal densities and configuration of the exploration network.

Study of the influence of climatic factors: the amount of precipitation, temperature, humidity, atmospheric electricity on the processes of bauxiformation and the establishment of the areas of their optimal manifestation;

Studying the role of the shape of the relief and its high-altitude stones on the bactic formation and the zoning of the territory of Guinea in geomorphological features;

Studying the effect of the composition of parents and tectonics to allocate the areas of the most favorable for bauximation as possible;

Study of the distribution of the main parameters of the mineralization - the power of the ore body, the contents of A1203, BUB?, RE203, TU2 and the silicon module inside bauxite deposits using methods of mathematical statistics;

Justification based on the inhomogeneities of bauxite deposits of optimal density and configuration of the exploration network.

The actual material based on the work. The work was carried out on materials of state geological funds of Guinea, its own documentation obtained in the process of personal participation in geological exploration work, as well as collected during special trips to Bokexiton areas bokeh, Kindy and Dubola.

The work uses:

Geological map of Guinea scale 1: 1 Ltd., LLC, compiled by geologists on "Barubeeology";

Physico-geographical map of Guinea scale 1: 1 OOO OOO;

Map of precipitation and vegetation Guinea scale 1: 1 Ltd. LLC;

Space photography Guinea;

Geological maps of boxite deposits debt and | Syntiura scale 1:50 OOO and 1: 200 LLC;

Plans of geological exploration works of bauxite deposits of the side of Bokeh, Kindy and Dubola scale 1:10 OOO and 1: 2 LLC;

The results of testing of 64 wells drilled in the fields of syntiura, debt and lighter. At the same time, more than 400 ordinary samples were used.

Based on the analysis of graphic materials, data of geological documentation and testing, the calculated characteristics that are used in the preparation of circuits, histograms and tables that substantiate the protected positions are compiled.

Approbation of work. The main provisions of the work were reported by the author at the National Geological Festival, in which all Geological Organizations Guinea were participating in the work, as well as repeatedly at meetings of the Scientific Faculty of the University of Concilia.

affecting the formation of rich in the content of alumina deposits.

The second chapter is devoted to the characteristic of geological factors of boxcofing in Guinea.

The third chapter provides a statistical analysis of the parameters of the mineralization inside bauxite deposits, their zonality is considered and the rationale for the most optimal densities and configuration of the exploration network is given. In the conclusion of the work, brief conclusions are given by IF the results of the studies conducted and are given practical

The dissertation was performed in the University of Konakrya under the scientific leadership of Avto Bortnikov A.Ya. And Viktorova G.G. Teachers MGG, working at present under the contract in Guinea. The dissertation is finalized in the Moscow State Geological Exploration Academy. Assistance in refinement of the thesis provided associate professors Sidorkov E.A. and Malyutin S.A.

The author is deeply grateful to his scientific leaders, as well as staff of the Department of Geoinformatics and Geology of mineral MGG for help and useful advice during the final finalization of the thesis.

Successful work on the dissertation contributed to the traditional ^ friendship between Russia and Guinea and, as a result of this, the colossal amount of work carried out by Russian geologists in Guinea. The author is grateful testifies to this.

Provide position. In dissertations are protected by three

provisions. The proof of the first position follow from the first and second challenges of the thesis, and the second and third from the third chapter.

First position. The deritment of the largest in stocks and rich in the content of alumina bauxite deposits to the triangle bokeh - Kindy - Tug is due to a unique combination of a complex of climate, geomorphological and geological factors favorable for bauxilite formation. Among climatic factors, a significant role belongs to atmospheric electrical tensions in the rainy season, the maximum of which falls on this area.

Second position. Bauxite deposits are characterized by the internal structure oriented internal structure and expressed in the uneven distribution of the main ore-forming components: AI203, FE203 and TJ2 in terms of and cutting.

Third position. Bauxite deposits with sections of geochemical heterogeneity, stretched according to the stretching, were more rational to explore a rectangular network, oriented in the same direction, with the aspect ratio of the cell calculated in each case case

1. "The use of geostatistical methods in the study of Guinean Boxitov deposits." Works of the University of Konakrya, 1998. (co-authors-A.Y. Katnikov, G.G.Viktorov.), 8 s.

2. "Geology and Natural Resources of the Dubol district (Guinea)" Proceedings of the University of Konakrya, 1998. (Cavators - G.G.Viktorov, M. Kava), 7 p.

3. "Introduction to geology". Tutorial. Edition of the University of Concilia, 1997, 106 p.

4. "Historical Geology" Tutorial. Edition of the University of Concilia, 1995, 112 p.

5. Chapter "Geology" in the study manual "Geology and Biology" for grade 9 secondary school. Edition of the National Institute of Pedagogical Studies (INRAP), Guinea, 1997, 21 p.

Guinea Bisau.

Kerouan ^ X cat-d "Ieuel

1 y200p? \\ "Shs and" 6 ¡4 0 | 5

^ - ed /< Бе/ла ^

/ / G "/) * / / 2 / Liberia" ^ Erenkore /

Placing the Boxite Squares of Guinea and Physico-Geographical Conditions of Boxitites

1 - isolated average annual temperature; 2 - isolated average annual precipitation (mm); 3 - Plateau Futa-Jalon (500-1000 m above sea level); 4 - high-rise marks; 5 - contour of bauxality; 6 - squares with estimated bauxite deposits; 7 - Boxitite deposits; 8 - Boxitite mining centers.

Appendix / g thesis r //

Statistical estimates of the chemical composition and capacity of Boxitites of the Guinea fields

according to sectional testing of core wells

Table 1

District Characteristics Statistical Parameters

N x s * v,% x Mj \\ x min r-xiuav-xinih a / hundred:

Side in L il 154/20 48,23 / 47.07 32,95 / 16.81,190 / 8.70 59.87 / 53.98 37,47 / 41.62 22,40 / 12.36 -0 ,fifteen/-

Wüh 152/20 1.23/133 1,21 / 0.64 89.76 / 60.15 4,43 / 4,03 0.27 / 0.62 4,16 / 3,41 2,251-

Feaö3 154/20 21.58 / 2344 72,76 / 37.70 39,52 / 26,19 41,13 / 31.07 4,98 / 12.92 36,15 / 18,14 3.00 / -

Tich 149/20 2.52 / 2.55 0.61 / 0.61 30,95 / 30.58 6.38 / 5.25 1.26/144 5,12 / 3,81 0.27 / -

P (M) - / 20 - / 7.7 - / 11.56 - / 44,15 - / 15.00 - / 3.00 - / 12.00 - / - 0.25

KChdiy Ahoj 155/22 48,12 / 48.00 23,43 / 17,31 10.06 / 8.66 59,87 / 56,65 37,47 / 40.24 22,40 / 16,41 0.20 / -

S1O2 155/22 2,23 / 2.23 1.23 / 0.61 50.00 / 34.97 4.68 / 3,87 0.24/126 4,44 / 2.61 0.40 / -

SHSHS 155/22 21.70 / 21.98 45,56 / 32.04 31,10 / 25.75 37,17 / 33,20 / 037 / 13,19 30,80 / 20.01 -0.47 / -

ty ....... 155/22 2.36 / 2.39 0.13 / 0.07 15.25 / 10,87 3.48 / 3.08 1.60 / 2.03 1.88 / 1.05 1.05 / -

P (M) - / 22 - / 7.13 - / 7.51 - / 38,42 - / 13.00 - / 3.00 - / 10.00 - / 1.05

DL1YU A1Y ........ 113/22 39.98 / 39.37 78,15 / 57.61 22.07 / 19.27 58,80 / 50.30 19,10 / 24.50 39, 70 / 25.80 -0.15 / -

SiOi 109/22 0.70 / 0.72 0.16 / 0.10 57.14 / 44.44 1.90 / 1,44 0.22 / 0.38 1.68 / 1.06 1,13 / -

Regude 113/22 35.38 / 36,56 148.35 / 106.50 34.04 / 28,22,64,30 / 57.70 14.00 / 22.07 50,30 / 35,63 0.39 / -

Tiö2 113/22 2.80 / 2.84 0.29 / 0.16 19.28 / 14.08 4.25 / 3,65 1.92 / 2.17 2.33 / 1.48 0.92 / -

P (M) 1 - / 22 - / 8.01 - / 4.84 - / 27.46 - / 11.90 - / 4.00 - / 7.90 - / - 1.27

Notes:

numerator - in sections, denominator - on the full exploration intersection N - the number of observations x max, x mjn - maximum and minimum values \u200b\u200bin

x - average arithmetic R \u003d xmax-Xmin - sampling

S2-dispersion A / a hundreds of asymmetry to the standard

asmetry

V,% - coefficient

variations Appendix / g Thesis U / 2

Distribution of the contents of the Ayosis on the detail section in the central hit the syntiura deposit

Annex / with the thesis

Existing Well Network

schedule of autocorrelation function of the contents of AK03

Latitude direction (3-c)

Meridional direction (S-Yu)

The proposed well network of the SZ direction "/ OZ 1 (P) MZ control" SZ

0.5 ol 0.3. 0.2 o, / o

200 "300 8 \u003d 250m

area statistically insignificant from them values \u200b\u200bof correlation coefficients

The graphs of autocorrelation functions of the contents of A1203 in the detail area in the central race of the syntiura deposit (I - the correlation radius, the limit distance on which the correlation bond in adjacent wells is preserved).

Annex to the thesis A / 3

Existing Well Network

oh Kommersant Suggested ° ^ Well Network

^ Rry - Island Relief

River Network

Orientation and geometry of the existing and proposed wells of wells on the central hit deposits

Syntiura

Annex to the thesis U3

Chapitre I: Conditions Geographiques De La Formation Des Gisements Bauxiteques en Guinee

Le But Visé Est L "Étude des Conditions De Formation Des Sols En Général et des Gisements De Bauxite en Particulier en Guinée.

Le Cours de Géologie Générale Nous Enseigne Pour QU "IL Y AIT FORMATION RÉSIDUELLE (SOL, CROûTE D" ALTÉRATION, ETC), IL FAUT:

L "EXISTENCE D" UNE ROCHE - Mère;

La Présence Des Organismes Végétaux Et Animaux

Un climat déterminé;

L "Âge des formations géologiques.

DANS CETTE PERSPECTIVE, IL NOUUS EST NÉCESSAIRE DE CONNATRE TUT D "ABORD LES CONDITIONS CLIMATIQUES FAVORISANT LA FORMATION DES GISEMENTS BAUXITIQUES.

Le Climat Est L "État Moyen des Conditions ATMOSPHÉRIQUES EN CERTAIN LIEU DU GLOBE TERRESTRE. DE PART SA SITUATION GÉOGRAPHIQUE ENTRE 7 ° 24" - 12 ° 32 "De Latitude Nord Entre 8 ° 00" - 14C45 "De Longitude de Ouest, La Guinée Appartient à DEUX Zones Climatiques:

la Zone Tropicale Pour La Majeure Partie Du Territoire et La Zone Subéquatoriale Au-Dessus Du 9ème Parallère Dans La Partie Sud-Est De La Guinée De Latitude Plus Basse Et Aux Montagnes Relavivement Élevées.

SELON AUBRÉVILLE LE FACTEUR CLIMATOLOGIQUE CAPITAL EST LA PLUVIOSITÉ EN TENANT COMPTE DE LA DURÉE DE LA SAISON SOCHE ET DE LA SAISON PLUVIEUSE. Le Rythme BioLogique Des Espèces Puissent Vivre Et Perpétuer Dans LEURS AIRES.

COMPTE-TENU DU RELIEF ET DU PAYSAGE, LA GUINÉE EST REPARTIE EN Quatre Régions Naturelles et, à ^ Chacune D "Elles CorreSpond UNE Sous-Zone Climatique à Savoir:

Le Climat Sub Guinéen; C "EST Le Climat Tropical Maritime En Basse-Guinée. Il Se Caractérise Par Une Température Moyenne Annuelle DE 23 ° À 25 ° C, Un Total Pluviométrique de 5,000 mm AUX ENVIRONS DE COVAH ET 2.100 MM À Kindia.

voir Tableau n ° ..............................

Le Climat Foutanien; c "est le climat tropical de montagne en Moyenne - Guinée Il se distingue par deux saisons de durée sensiblement avec une pluviométrie annuelle variant de 2.000 mm sur le versant Occidental exposé à la mousson océanique humide à 1600 mm sur le versant Oriental tourné vers la. Haute - Guinée.

Les Températures Sont ADOUCIES PAR LE RELIEF. Des Tableaux de pluviosité, D "Humidité Relative Et De Température Pour Les Quatre Régions Naturelles Seront Donnés en Fin du Paragraphe.

Le Climat Sud - Soudanien; C "EST Le Climat Soudanien En Haute - Guinée. Il Totalise Une Quantité Annuelle De Pluie De L" Ordre de 1500 à 1100 mm Avec Une Température Élevée, Principalement Vers La Fin de La Saison Sèche (Mars - Avril).

Le Climat Subéquatorial; c "est le climat équatorial Guinéen en Guinée -. Forestière Il se caractérise pour longue saison pluvieuse de 8 à 10 mois selon la situation en latitude et en altitude La pluviométrie annuelle varie de 1600 à 2800 mm et la température moyenne annuelle est de 24. ° À 26 ° C.

Nous Présentons Dans Les Pages Suivantes.

1 - Un Tableau des Stations Météorologiques de la Guinée

2 - Un Tableau de PluvioMétrie de la Guinée

3 - Un Tableau D "Humidité Relative

4 - Un Tableau des températures.

La Plaine Côtière et Son Arrière - Pays Portent Le Nom De Basse-Guinée Ou Guinée-Maritime. Ainsi, de l "océan vers l" intérieur on passe successivement du littoral à une plaine submersible puis à une plaine non inondable avant de buter contre l "écran montagneux des contreforts occidentaux du Fouta-Djallon. Le littoral Atlantique de la Guinée se caractérise par Un Tracé Découpé Comprenant des îles et îlots, des Secteurs Rectilignnes, En Cap, Presqu "île Ou Baie. Le Cap Verga et La Presqu "île du Kaloum Sont Les Deux Principals Avancées Du Continent Sur La Mer et La Principles Avancées Du Continent Sur La Mer et La Principle Baie Est Celle de Sangréa à Dubreka.

La Plaine Côtière S "Élargit AU NORD ET AU SUD. EN RAISON DE LA FAIBLESSE DE L" ALTITUDE ET De La Remontée De La Marée, La Plaine Côtière Est Généralement Submersible à L "Exception Des Cordons Littoraux.

VERS L "INTÉRIEUR DU Continent L" Altitude Augmente Rendant Impossible Toute Inondation Par Les Eaux Marines. C "EST LA ZONE DES PLAINES Exondées.

Les Plaines de La Basse - Guinée Sont Brusquement Dominées à l "Est Par Un Écran Montagneux Sous Forme D" Une Falaise Verticale Qui Constitue La Retombée Occidentale du Massif du Fouta-Djallon.

Les Plus Spectaculaires De Ces Contreme Sont Les Massifs de Benna, Kakoulima, Balan, Gangan.

Un Massif Ancien Accidenté, Situé Au Center Ouest De La Guinée, Le Massif du Fouta-Djallon. IL Occupe Environment 80.000 KM2 ET Culmine Au Mont Loura (1538 m). IL EST DISPOSÉ EN

TABFEA-J N °< 1: Stations Météorologiques de la Guinée

Station Latitude Longitude Altitude

Benty 09 ° 10 "N 13 ° 33" W 100

Beyla 08 ° 41 "N 08 ° 39" W 695

BISSIKR1MA 10 ° 51 "N 10 ° 55" W 400

Boffa 10 ° 21 "N 14 ° 26" W 30

Boke 10 ° 56 "ñ 14 ° 19" W 69

Conakry Aero. 09 ° 34 "N 13 ° 37" W 5

Coyah 09 ° 42 "N 13 ° 23" W 20

Dabola 10 ° 45 "N 11 WW 438

Dalaba 10 ° 43 "N 12 ° 15" W 1202

DinguirayE 11 ° 18 "N 10 ° 43" W 490

Ditinn 10 ° 53 "N 12 ° 11" W 750

Dubreka 09 ° 47 "N í3 ° 28" W 15

Faranah 10 ° 02 "N 10 ° 42" W 340

Forecariah 09 ° 26 "N 13 ° 06" W 47

Gaoual 11 ° 17 "N 13 ° 12" W 100

Gueckedou 08 ° 33 "N 10 ° 09" W 435

Kankan to ° 23 "N 09 ° 18" W 377

Kindia 10 ° 03 "N 12 ° 52" W 459

K! SS! DOUGOU 09 ° 11 "N 10 ° 06" W 450

KourousSa 10 ° 39 "N 09 ° 53" W 372

Labe 11 ° 19 "N 12 ° 18" W 1025

Macenta 08 ° 32 "N 09 ° 28" W 543

Mali 12 ° 08 "N 12 ° 18" W 1464

MAM.OU 10 ° 22 "N 12 ° 04" W 785

N "zerekore 07 ° 45" n 08 ° 17 "W 520

Pita 11 ° 04 "N 12 ° 24" W 965

Seredou 10 ° 43 "N 12 ° 16" W 850

Saraboidq 12 ° 24 "N 13 ° 31" W -

Siguiri 11 ° 26 "N 09 ° 10" W 361

Tamara 09 ° 27 "N IS-SO" W, 90

Telemele 10 ° 56 "N 13 ° 00" W 650

TOLO 10 ° 50 "N 12 ° 00" W 750

TOUGUE 11 ° 26 "N 11 ° 40" W 868

Victoria 10 ° 49 "N 14 ° 32" W 7

Youkoundkoun 12 ° 32 "N 09 ° 16" W -Â2_

Tableau NC 2: Tableau de Pluviométries Moyennes Mensuelles Et Annuelles EN

1 Station! Il HT IV V V! VLI VLIL IX X XI XII Annuelle

Macenta 15.5 55.2 146.9 177.6 270.5 281.0 480.0 536.1 431.7 266,3,176,7 53,6,291,1

33 ANS 1.2 3.9 10.6 14.7,51,55,52,21,22,29,22,21,23 3.4 .173.1

Seredou 11.5 37.7,17.0 175.6 202.4 215.8 378.8 594.0 440.5 229.7 135.6 41,1,579,7

c. AI ■.

c 5 U N "Zerekore 19.2 41.1 126.5 148.7 177.8 2